Blanco Fracture Zone

E73487

The Blanco Fracture Zone is a major transform fault and fracture zone in the northeast Pacific Ocean that offsets and separates segments of the Juan de Fuca and Pacific tectonic plates.


Statements (35)

Predicate Object
instanceOf fracture zone
tectonic feature
transform fault
associatedWith Cascadia Subduction Zone
surface form: Cascadia subduction zone

Gorda Ridge
Juan de Fuca Ridge
crustType oceanic crust
geologicalAge Cenozoic
geologicalProcess seafloor spreading offset
hasFeature earthquake activity
hasOrientation approximately east–west
hasResearchField marine geology
plate tectonics
seismology
hazardType seismic hazard
isPartOf Cascadia Subduction Zone
surface form: Juan de Fuca–Pacific plate boundary system
isUnder Pacific Ocean seafloor
linkedTo regional tectonic deformation in the Cascadia margin
locatedIn eastern North Pacific Ocean
surface form: northeast Pacific Ocean
locatedOffCoastOf Oregon
Northern California
surface form: northern California
motionType strike-slip
namedAfter Blanco Transform
ocean Pacific Ocean
offsets segments of the Juan de Fuca Plate
segments of the Pacific Plate
partOf plate boundary system of the northeast Pacific
plateBoundaryBetween Juan de Fuca Plate
Pacific Plate
relativePlateMotion right-lateral
separates Juan de Fuca Plate
Pacific Plate
tectonicRegion Cascadia
surface form: Cascadia region
tectonicRole accommodates differential motion between the Juan de Fuca and Pacific plates
tectonicSetting plate boundary between the Juan de Fuca Plate and the Pacific Plate

Referenced by (3)

Full triples — surface form annotated when it differs from this entity's canonical label.

Gorda Ridge connectedTo Blanco Fracture Zone
Gorda Plate northernBoundaryFeature Blanco Fracture Zone
Juan de Fuca Ridge terminatesNear Blanco Fracture Zone